4.6 Article

Investigating the Elusive Nature of Atomic O from CO2 Dissociation on Pd(111): The Role of Surface Hydrogen

期刊

JOURNAL OF PHYSICAL CHEMISTRY C
卷 126, 期 18, 页码 7870-7879

出版社

AMER CHEMICAL SOC
DOI: 10.1021/acs.jpcc.2c00976

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资金

  1. DOE Office of Science [DE-SC0012704]
  2. division of Chemical Science, Geoscience, and Bioscience, Office of Basic Energy Science of the US Department of Energy (DOE) [DE-SC0012704]
  3. Scientific Data and Computing Center, a component of the Computational Science Initiative, at BNL [DE-SC0012704]
  4. National Science Foundation grant [1531492]
  5. Direct For Computer & Info Scie & Enginr
  6. Office of Advanced Cyberinfrastructure (OAC) [1531492] Funding Source: National Science Foundation

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Through experimental and computational studies, it was found that CO2 dissociation on the Pd(111) surface primarily leads to adsorbed CO, while atomic O is only observed at higher temperatures. The presence of background H-2 promotes the dissociation of CO2, resulting in the formation of adsorbed CO and removal of O. These findings offer new opportunities for controlling CO2 hydrogenation catalysis.
CO2 dissociation is a key step in CO2 conversion reactions to produce value-added chemicals typically through hydrogenation. In many cases, the atomic O produced from CO2 dissociation can potentially block adsorption sites or change the oxidation state of the catalyst. Here, we used ambient pressure X-ray photoelectron spectroscopy (AP-XPS) and density functional theory (DFT) calculations to investigate the presence of surface species from the dissociation of CO2 on Pd(111). AP-XPS results show that CO2 was dissociated to produce adsorbed CO, but dissociated atomic O was not observed at room temperature. We were only able to observe atomic O when CO2 was introduced at 500 K. Further investigations of O-covered Pd(111) revealed that chemisorbed O could be easily removed by low pressures of CO and H-2. Notably, the effect of H-2 is quite prominent since it could react with chemisorbed O at a pressure as low as 2 x 10(-9) Ton, and the presence of H-2 at ambient pressure prevented CO2 dissociation. DFT calculations showed that in the presence of background H-2, facile CO2 dissociation took place via the reverse water-gas shift (rWGS) reaction, which resulted in the formation of adsorbed CO and removal of O by H-2. DFT also identified the possible variation of surface species on simultaneous exposure of CO2 and H-2 over Pd(111) depending on temperature and pressure, which opens alternative opportunities to tune the CO2 hydrogenation catalysis by controlling the reaction conditions.

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